Abstract
Abstract We acquired coincident wide-angle and multi-channel seismic reflection data along four profiles perpendicular to the Kyushu-Palau Ridge (KPR) between 15°N and 20°N on the Philippine Sea plate. The crustal thickness beneath the KPR, which is a remnant arc created in the Late Eocene, varies along the strike from 8 to approximately 20 km and is always thicker than the adjacent oceanic crust of the West Philippine Basin to the west and the Parece Vela Basin to the east. The thickest crust among the four profiles, which is primarily due to a thickening of the lower crust, is found where the KPR adjoins Oki-no-Tori-Shima Island. There is no clear evidence of the thick (>5 km) middle crustal layer with a P-wave velocity of 6.0–6.5 km/s that has been inferred beneath the conjugate rifted counterpart of the Izu-Ogasawara(Bonin)-Mariana Island-arc. Our results suggest that the crust of the KPR at 15–21°N represents a less mature island arc crust relative to that further north along the ridge where a mid-crustal layer of 6 km/s has been reported.
Highlights
The Kyushu-Palau Ridge (KPR) is a bathymetric high, extending north-south near the center of the Philippine Sea (Fig. 1)
Due to the trade off between the crustal thickness of the KPR and Pn velocity beneath the ridge, it is difficult to determine the depth of the Moho with any precision
Significant reflections indicating a middle/lower crust boundary in the KPR crust were not identified more than two continuous ocean bottom seismographs (OBS)
Summary
The Kyushu-Palau Ridge (KPR) is a bathymetric high, extending north-south near the center of the Philippine Sea (Fig. 1). Due to the trade off between the crustal thickness of the KPR and Pn velocity beneath the ridge, it is difficult to determine the depth of the Moho with any precision.
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